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<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal">Xu, Y., Lin, X., Sun, Q.-B., Xiao, H.-W., Xiao, H., & Xiao, H.-Y. (2024). Elaborating the atmospheric transformation of combined and free amino acids from the perspective of observational studies. <i>Journal of Geophysical Research: Atmospheres</i>,
129, e2024JD040730. <a href="https://doi.org/10.1029/2024JD040730" target="_blank">https://doi.org/10.1029/2024JD040730</a>. <o:p></o:p></p>
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<p class="MsoNormal"><b>Abstract. </b>Proteinaceous matter (PrM) is a substantial component of bioaerosols. Although numerous studies have examined the characteristics and sources of PrM in the atmosphere, its interactions with atmospheric oxidants remain uncertain.
A 1-year observation of PrM characteristics in PM<sub>2.5</sub> was performed in both urban Nanchang (eastern China) and suburban Guiyang (southwestern China), respectively. Glycine was the dominant free amino acid (FAA) species in urban Nanchang. In contrast,
proline dominated both total free amino acids (FAAs) and total combined amino acids (CAAs) in suburban Guiyang. We found that oxidative degradation can significantly promote the release of FAAs, especially glycine, from CAAs in Nanchang. The controlled experiment
on protein oxidation by hydroxyl radical suggested that the contribution of free glycine to the total FAA fraction tended to increase during the oxidative degradation of CAAs, supporting the predominance of glycine in FAAs in Nanchang and most previous observations.
The composition of FAAs was mainly influenced by primary sources in suburban Guiyang with weak atmospheric degradation of PrM. These results suggest that the degradation of aerosol PrM by atmospheric oxidants can be responsible for the difference in FAA composition
between the biosphere and the atmosphere, and also imply that the oxidative degradation of aerosol PrM may be a potential source of secondary organic nitrogen compounds in aerosols. Thus, this study can improve the current understanding of the composition
characteristics of PrM in the biosphere and the atmosphere, as well as the liquid phase reactions of proteinaceous compounds with atmospheric oxidants.<o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal"><a href="https://sites.google.com/site/pamwiki/publications-using-other-oxidation-flow-reactors">PAM Wiki - Publications Using Other Oxidation Flow Reactors (google.com)</a><o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal"><span style="mso-ligatures:none">Andrew Lambe<o:p></o:p></span></p>
<p class="MsoNormal"><span style="mso-ligatures:none">Principal Scientist<o:p></o:p></span></p>
<p class="MsoNormal"><span style="mso-ligatures:none">Aerodyne Research, Inc. <o:p>
</o:p></span></p>
<p class="MsoNormal"><o:p> </o:p></p>
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